Titlebook: Reading the Archive of Earth’s Oxygenation; Volume 1: The Palaeo Victor A. Melezhik,Anthony R. Prave,Eero J. Hanski Book 2013 Springer-Verl

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3.4 Evolution of the Palaeoproterozoic (2.50–1.95 Ga) Non-orogenic Magmatism in the Eastern Part of rifting of the Archaean cratons of the shield and the commencement of the Svecofennian orogenic events, covering a prolonged inter-orogenic period from c. 2.5 to 1.95 Ga. The focus is on igneous events that took place on and in the Karelian and Kola cratons. These cratons were stabilised by c. 2.6 G

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4.2 The Pechenga Greenstone Belt through Norway to Finland and back to Norway. About 600 km of that belt occurs in the Russian part of the Fennoscandian Shield and is commonly called the Pechenga-Imandra/Varzuga Greenstone Belt. In order to embrace the entirety of the belt, Melezhik and Sturt (1994) introduced the term Polmak-Pasv

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4.3 The Onega Basint formed initially as a Palaeoproterozoic rift basin and contains a c. 2440–1980 Ma, low metamorphic-grade, volcano-sedimentary succession that has served as a stratotype area for the establishment of formal lithostratratigraphic subdivision of the Palaeoproterozoic of the former Soviet Union (e.g.

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Victor A. Melezhik,Anthony R. Prave,Eero J. HanskiEstablishment of a well-characterized, well-dated and well-archived succession of rocks for the period of 2500-2000 Ma.Documentation of the changes in the biosphere and the geosphere associated with t

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978-3-662-52201-1Springer-Verlag Berlin Heidelberg 2013

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Reading the Archive of Earth’s Oxygenation978-3-642-29682-6Series ISSN 1863-4621 Series E-ISSN 1863-463X

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